Vegetation and environmental conditions in the Doñana Natural Park coastal area (SW Iberia) at the beginning of the last glacial cycle
Detailed reconstructions of the vegetation of Iberia during the last glacial inception are rare due to the limited number of terrestrial sites recording this period. Active retreat of El Asperillo cliff, located on the Atlantic coast of southwestern Iberia, has exposed a fossil organic level dating...
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Veröffentlicht in: | Quaternary research 2011-01, Vol.75 (1), p.205-212 |
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description | Detailed reconstructions of the vegetation of Iberia during the last glacial inception are rare due to the limited number of terrestrial sites recording this period. Active retreat of El Asperillo cliff, located on the Atlantic coast of southwestern Iberia, has exposed a fossil organic level dating back to one of the early stades of the last glacial cycle. Pollen and macrofossil analyses from this site show that the Doñana area was covered mainly by steppic vegetation; temperate trees survived the coldest periods, albeit in reduced numbers. Mediterranean taxa are extremely reduced, in contrast with other dry areas of southern Iberia over this time span. This vegetation suggests cold and arid climatic conditions, in accordance with paleoclimatic reconstructions based on several Atlantic marine cores. |
doi_str_mv | 10.1016/j.yqres.2010.08.009 |
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Active retreat of El Asperillo cliff, located on the Atlantic coast of southwestern Iberia, has exposed a fossil organic level dating back to one of the early stades of the last glacial cycle. Pollen and macrofossil analyses from this site show that the Doñana area was covered mainly by steppic vegetation; temperate trees survived the coldest periods, albeit in reduced numbers. Mediterranean taxa are extremely reduced, in contrast with other dry areas of southern Iberia over this time span. 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Active retreat of El Asperillo cliff, located on the Atlantic coast of southwestern Iberia, has exposed a fossil organic level dating back to one of the early stades of the last glacial cycle. Pollen and macrofossil analyses from this site show that the Doñana area was covered mainly by steppic vegetation; temperate trees survived the coldest periods, albeit in reduced numbers. Mediterranean taxa are extremely reduced, in contrast with other dry areas of southern Iberia over this time span. This vegetation suggests cold and arid climatic conditions, in accordance with paleoclimatic reconstructions based on several Atlantic marine cores.</description><subject>Aridity</subject><subject>Biogeography</subject><subject>Coastal areas</subject><subject>Coastal geomorphology</subject><subject>Cold stage</subject><subject>Dating</subject><subject>Drying</subject><subject>Fossil wood</subject><subject>Fossils</subject><subject>Late Pleistocene</subject><subject>Macrofossil</subject><subject>Marine</subject><subject>Myrica</subject><subject>Pollen</subject><subject>Reconstruction</subject><subject>Recording</subject><subject>Vegetation</subject><issn>0033-5894</issn><issn>1096-0287</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNqFkEuO1DAQhi0EEs3ACdh4ByzSVDqJ7SxYoBkeI40AidfSqtiV4CZtz9jukfoEnIczcDGc7lnDyqqq73epPsae1rCuoRYvt-vDTaS03kDpgFoD9PfYqoZeVLBR8j5bATRN1am-fcgepbSFUm8UrNivbzRRxuyC5-gtJ3_rYvA78hlnboK3bpkl7jzPP4hfhD-_0SP_gHkfC_EJ48-CYVpwjIT8-efv_HKg6PAFx3wMDTQ5752feBiPjbnwfJrRuGXJwcz0mD0YcU705O49Y1_fvvly_r66-vju8vz1VYUttLlSkuTQytEY6A1JNcDQIFghhJVCDGRRNlaNNQojNkrV1GBX950dxAhilKo5Y89O_17HcLOnlPXOJUPzjJ7CPmkloJF9C10hmxNpYkgp0qivo9thPOga9GJdb_XRul6sa1C6WC-pV6cUlSNuHUWdjCNvyLpIJmsb3H_y3d1W3A3R2Yn0NuyjL07-mfsLmPOgbg</recordid><startdate>201101</startdate><enddate>201101</enddate><creator>Morales-Molino, César</creator><creator>Postigo-Mijarra, José María</creator><creator>García-Antón, Mercedes</creator><creator>Zazo, Cari</creator><general>Cambridge University Press</general><general>Elsevier Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>201101</creationdate><title>Vegetation and environmental conditions in the Doñana Natural Park coastal area (SW Iberia) at the beginning of the last glacial cycle</title><author>Morales-Molino, César ; Postigo-Mijarra, José María ; García-Antón, Mercedes ; Zazo, Cari</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a404t-87e7b47fcc09ce78b0b3a0d666d766beda73d8f1a6c62881e3a5195db6f06f783</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Aridity</topic><topic>Biogeography</topic><topic>Coastal areas</topic><topic>Coastal geomorphology</topic><topic>Cold stage</topic><topic>Dating</topic><topic>Drying</topic><topic>Fossil wood</topic><topic>Fossils</topic><topic>Late Pleistocene</topic><topic>Macrofossil</topic><topic>Marine</topic><topic>Myrica</topic><topic>Pollen</topic><topic>Reconstruction</topic><topic>Recording</topic><topic>Vegetation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Morales-Molino, César</creatorcontrib><creatorcontrib>Postigo-Mijarra, José María</creatorcontrib><creatorcontrib>García-Antón, Mercedes</creatorcontrib><creatorcontrib>Zazo, Cari</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Quaternary research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Morales-Molino, César</au><au>Postigo-Mijarra, José María</au><au>García-Antón, Mercedes</au><au>Zazo, Cari</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Vegetation and environmental conditions in the Doñana Natural Park coastal area (SW Iberia) at the beginning of the last glacial cycle</atitle><jtitle>Quaternary research</jtitle><addtitle>Quat. res</addtitle><date>2011-01</date><risdate>2011</risdate><volume>75</volume><issue>1</issue><spage>205</spage><epage>212</epage><pages>205-212</pages><issn>0033-5894</issn><eissn>1096-0287</eissn><abstract>Detailed reconstructions of the vegetation of Iberia during the last glacial inception are rare due to the limited number of terrestrial sites recording this period. Active retreat of El Asperillo cliff, located on the Atlantic coast of southwestern Iberia, has exposed a fossil organic level dating back to one of the early stades of the last glacial cycle. Pollen and macrofossil analyses from this site show that the Doñana area was covered mainly by steppic vegetation; temperate trees survived the coldest periods, albeit in reduced numbers. Mediterranean taxa are extremely reduced, in contrast with other dry areas of southern Iberia over this time span. This vegetation suggests cold and arid climatic conditions, in accordance with paleoclimatic reconstructions based on several Atlantic marine cores.</abstract><cop>New York, USA</cop><pub>Cambridge University Press</pub><doi>10.1016/j.yqres.2010.08.009</doi><tpages>8</tpages></addata></record> |
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subjects | Aridity Biogeography Coastal areas Coastal geomorphology Cold stage Dating Drying Fossil wood Fossils Late Pleistocene Macrofossil Marine Myrica Pollen Reconstruction Recording Vegetation |
title | Vegetation and environmental conditions in the Doñana Natural Park coastal area (SW Iberia) at the beginning of the last glacial cycle |
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